Green's theorem

Green's theorem
In vector calculus, Green's theorem relates a line integral around a simple closed curve to a double integral over the plane region bounded by . It is the two-dimensional special case of Stokes' theorem.
Theorem
Let be a positively oriented, piecewise smooth, simple closed curve in a plane, and let be the region bounded by . If and are functions of defined on an open region containing and have continuous partial derivatives there, then
where the path of integration along is anticlockwise.
In physics, Green's theorem finds many applications. One is solving two-dimensional flow integrals, stating that the sum of fluid outflowing from a volume is equal to the total outflow summed about an enclosing area. In plane geometry, and in particular, area surveying, Green's theorem can be used to determine the area and centroid of plane figures solely by integrating over the perimeter.
Proof when D is a simple region
The following is a proof of half of the theorem for the simplified area D, a type I region where C1 and C3 are curves connected by vertical lines (possibly of zero length). A similar proof exists for the other half of the theorem when D is a type II region where C2 and C4 are curves connected by horizontal lines (again, possibly of zero length). Putting these two parts together, the theorem is thus proven for regions of type III (defined as regions which are both type I and type II). The general case can then be deduced from this special case by decomposing D into a set of type III regions.
If it can be shown that
and
are true, then Green's theorem follows immediately for the region D. We can prove easily for regions of type I, and for regions of type II. Green's theorem then follows for regions of type III.
Assume region D is a type I region and can thus be characterized, as pictured on the right, by
where g1 and g2 are continuous functions on . Compute the double integral in:
Now compute the line integral in. C can be rewritten as the union of four curves: C1, C2, C3, C4.
With C1, use the parametric equations: x = x, y = g1(x), a ≤ x ≤ b. Then
With C3, use the parametric equations: x = x, y = g2(x), a ≤ x ≤ b. Then
The integral over C3 is negated because it goes in the negative direction from b to a, as C is oriented positively (anticlockwise). On C2 and C4, x remains constant, meaning
Therefore,
Combining with, we get for regions of type I. A similar treatment yields for regions of type II. Putting the two together, we get the result for regions of type III.
Proof for rectifiable Jordan curves
We are going to prove the following
We need the following lemmas whose proofs can be found in:
Now we are in position to prove the theorem:
Proof of Theorem. Let be an arbitrary positive real number. By continuity of , and compactness of , given , there exists such that whenever two points of are less than apart, their images under are less than apart. For this , consider the decomposition given by the previous Lemma. We have
Put .
For each , the curve is a positively oriented square, for which Green's formula holds. Hence
Every point of a border region is at a distance no greater than from . Thus, if is the union of all border regions, then ; hence , by Lemma 2. Notice that
This yields
We may as well choose so that the RHS of the last inequality is
The remark in the beginning of this proof implies that the oscillations of and on every border region is at most . We have
By Lemma 1(iii),
Combining these, we finally get
for some . Since this is true for every , we are done.
Validity under different hypotheses
The hypothesis of the last theorem are not the only ones under which Green's formula is true. Another common set of conditions is the following:
The functions are still assumed to be continuous. However, we now require them to be Fréchet-differentiable at every point of . This implies the existence of all directional derivatives, in particular , where, as usual, is the canonical ordered basis of . In addition, we require the function to be Riemann-integrable over .
As a corollary of this, we get the Cauchy Integral Theorem for rectifiable Jordan curves:
Multiply-connected regions
Theorem. Let be positively oriented rectifiable Jordan curves in satisfying
where is the inner region of . Let
Suppose and are continuous functions whose restriction to is Fréchet-differentiable. If the function
is Riemann-integrable over , then
Relationship to Stokes' theorem
Green's theorem is a special case of the Kelvin–Stokes theorem, when applied to a region in the -plane.
We can augment the two-dimensional field into a three-dimensional field with a z component that is always 0. Write F for the vector-valued function . Start with the left side of Green's theorem:
The Kelvin–Stokes theorem:
The surface is just the region in the plane , with the unit normal defined (by convention) to have a positive z component in order to match the "positive orientation" definitions for both theorems.
The expression inside the integral becomes
Thus we get the right side of Green's theorem
Green's theorem is also a straightforward result of the general Stokes' theorem using differential forms and exterior derivatives:
Relationship to the divergence theorem
Considering only two-dimensional vector fields, Green's theorem is equivalent to the two-dimensional version of the divergence theorem:
where is the divergence on the two-dimensional vector field , and is the outward-pointing unit normal vector on the boundary.
To see this, consider the unit normal in the right side of the equation. Since in Green's theorem is a vector pointing tangential along the curve, and the curve C is the positively oriented (i.e. anticlockwise) curve along the boundary, an outward normal would be a vector which points 90° to the right of this; one choice would be . The length of this vector is So
Start with the left side of Green's theorem:
Applying the two-dimensional divergence theorem with , we get the right side of Green's theorem:
Area calculation
Green's theorem can be used to compute area by line integral. The area of a planar region is given by
Choose and such that , the area is given by
Possible formulas for the area of include
History
It is named after George Green, who stated a similar result in an 1828 paper titled An Essay on the Application of Mathematical Analysis to the Theories of Electricity and Magnetism. In 1846, Augustin-Louis Cauchy published a paper stating Green's theorem as the penultimate sentence. This is in fact the first printed version of Green's theorem in the form appearing in modern textbooks. Bernhard Riemann gave the first proof of Green's theorem in his doctoral dissertation on the theory of functions of a complex variable.
See also
Method of image charges – A method used in electrostatics that takes advantage of the uniqueness theorem (derived from Green's theorem)
Shoelace formula – A special case of Green's theorem for simple polygons
References
Further reading
External links
Green's Theorem on MathWorld
Theorems in calculus
Articles containing proofs